Weather Alert in Colorado
High Wind Warning issued March 11 at 11:50PM MDT until March 13 at 12:00PM MDT by NWS Denver CO
AREAS AFFECTED: South and East Jackson/Larimer/North and Northeast Grand/Northwest Boulder Counties Above 9000 Feet; South and Southeast Grand/West Central and Southwest Boulder/Gilpin/Clear Creek/Summit/North and West Park Counties Above 9000 Feet; Larimer and Boulder Counties Between 6000 and 9000 Feet
DESCRIPTION: * WHAT...West winds 35 to 50 mph with gusts 80 to 100 mph expected. * WHERE...Rocky Mountain National Park and the Medicine Bow Range, The Mountains of Summit County, the Mosquito Range, the Indian Peaks, and The Northern Front Range Foothills. * WHEN...From 4 AM Thursday to noon MDT Friday. * IMPACTS...Damaging winds may blow down trees and power lines, and scattered power outages are possible. Travel will be difficult, especially for high profile vehicles. This includes U.S. 40 over Berthoud Pass, I-70 from Golden to the Eisenhower Tunnel, and the Peak to Peak Highway. Strong winds may lead to rapid growth of any new fires, particularly below 7,500 ft.
INSTRUCTION: Drivers of high profile vehicles should consider delaying travel until winds subside Friday afternoon. People are urged to secure loose objects that could be blown around or damaged by the wind.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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